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1. Tibetan Plateau

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   During the summer months, intense solar insolation heats the vast, dry surface area of the Plateau. This leads to the rapid expansion and ascent of the overlying air mass, generating a persistent, deep thermal low-pressure system. This low pressure drives the inflow of warm, moist air from the Indian Ocean and the Bay of Bengal, forming the core of the Asian Monsoon [1].
   Paradoxically, the Plateau’s influence is not solel…